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甘肃北山地区牛圈子蛇绿岩的形成时代及地质意义

武鹏 王国强 李向民 余吉远 康磊

地质通报2012,Vol.31Issue(12):2032-2037,6.
地质通报2012,Vol.31Issue(12):2032-2037,6.

甘肃北山地区牛圈子蛇绿岩的形成时代及地质意义

The age of Niujuanzi ophiolite in Beishan area of Gansu Province and its geological significance

武鹏 1王国强 1李向民 2余吉远 1康磊1

作者信息

  • 1. 中国地质调查局西安地质调查中心,陕西西安710054
  • 2. 长安大学地球科学与资源学院,陕西西安710064
  • 折叠

摘要

Abstract

In order to study the age of Xichangjing-Niujuanzi-Hongliuhe ophiolite belt in Beishan area of Gansu Province, the authors conducted zircon LA—ICP—MS U—Pb dating of gabbro from this ophiolite belt. The result shows that the weighted average 206Pb/238U age of this ophiolite is 446.5 Ma±4Ma, suggesting late Ordovician. In combination with previous researches, the authors hold that Niujuanzi ophiolite and Hongliuhe ophiolite should be the products of early Paleozoic Ocean evolution. This study is of important significance for the study of tectonic evolution in Beishan area during early Paleozoic period.

关键词

甘肃北山/LA-ICP-MS锆石U-Pb定年/牛圈子蛇绿岩

Key words

Beishan area of Gansu /LA-ICP-MS zircon U-Pb dating/Niujuanzi ophiolite

分类

天文与地球科学

引用本文复制引用

武鹏,王国强,李向民,余吉远,康磊..甘肃北山地区牛圈子蛇绿岩的形成时代及地质意义[J].地质通报,2012,31(12):2032-2037,6.

基金项目

中国地质调查局地质调查项目《北山-祁连成矿带地质矿产综合研究》(编号:1212011085077)、《北祁连成矿带成矿条件研究与找矿靶区优选》(编号:1212010818090) (编号:1212011085077)

地质通报

OA北大核心CSCDCSTPCD

1671-2552

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